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Morphology, Genesis, and Distribution of Nanometer-Scale Pores in Siliceous Mudstones of the Mississippian Barnett Shale

机译:密西西比巴尼特页岩硅质泥岩中纳米级孔隙的形态,成因和分布

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摘要

Research on mudrock attributes has increased dramatically since shale-gas systems have become commercial hydrocarbon production targets. One of the most significant research questions now being asked focuses on the nature of the pore system in these mudrocks. Our work on siliceous mudstones from the Mississippian Barnett Shale of the Fort Worth Basin, Texas, shows that the pores in these rocks are dominantly nanometer in scale (nanopores). We used scanning electron microscopy to characterize Barnett pores from a number of cores and have imaged pores as small as 5 nm. Key to our success in imaging these nanopores is the use of Ar-ion-beam milling; this methodology provides flat surfaces that lack topography related to differential hardness and are fundamental for high-magnification imaging.
机译:页岩气系统成为商业化油气生产目标以来,对泥岩属性的研究已大大增加。现在被问到的最重要的研究问题之一集中在这些 孔雀中的毛孔系统的性质。我们对得克萨斯州沃思堡盆地密西西比州 Barnett页岩的硅质泥岩的研究表明,这些岩石中的 孔主要是纳米级(纳米孔)。 > 我们使用扫描电子显微镜从许多核中表征了Barnett 孔,并成像了小至5nm的孔。我们成功地对这些纳米孔成像的关键是 使用Ar离子束研磨;此方法提供了平坦的表面 ,该表面不具有与硬度差有关的形貌,并且是 基本的高倍率成像。

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  • 来源
    《Journal of Sedimentary Research》 |2009年第12期|848-861|共14页
  • 作者单位

    Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, U.S.A. bob.loucks@beg.utexas.edu;

    Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, U.S.A.;

    Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, U.S.A.;

    Energy Institute, Texas Christian University, Fort Worth, Texas 76109, U.S.A.;

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